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Trace element partitioning in basaltic systems as a function of oxygen fugacity

Abstract:

Along with temperature, pressure and melt chemistry, magmatic oxygen fugacity (fO2) has an important influence on liquid and solid differentiation trends and melt structure. To explore the effect of redox conditions on mineral stability and mineral-melt partitioning in basaltic systems we performed equilibrium, one-atmosphere experiments on a picrite at 1200–1110 °C with fO2 ranging from NNO-4 log units to air. Clinopyroxene ...

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Publication status:
Published
Peer review status:
Peer reviewed

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Publisher copy:
10.1007/s00410-023-02069-x

Authors


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Institution:
University of Oxford
Division:
MPLS
Department:
Earth Sciences
Role:
Author
ORCID:
0000-0001-7263-8925



Publisher:
Springer
Journal:
Contributions to Mineralogy and Petrology More from this journal
Volume:
178
Issue:
12
Article number:
95
Publication date:
2023-11-27
Acceptance date:
2023-10-05
DOI:
EISSN:
1432-0967
ISSN:
0010-7999


Language:
English
Keywords:
Pubs id:
1570506
Local pid:
pubs:1570506
Deposit date:
2023-11-25

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